经过气候变化的花岩和土壤可以容纳含有依赖兰坦化的甲基转化酶的微生物
Marcos Y Voutsinos1,2, Jacob A West-Roberts3, Rohan Sachdeva4
1School of Geography, Earth and Atmospheric Sciences, The University of Melbourne, Melbourne, VIC, Australia.
BMC biology
|February 18, 2024
概括
经过气候变化的花岩中的微生物利用兰坦化物进行甲醇代谢,帮助酸盐释放和土壤形成. 这项研究确定了关键的有机体和基因途径,涉及岩土转化.
科学领域:
- 地质微生物学的生物.
- 环境微生物学 环境微生物学
- 生物地质化学生物地质化学
背景情况:
- 酸盐对生命至关重要,但通常被锁定在不溶性酸盐矿物质中.
- 微生物在溶解这些矿物质和利用兰坦化物中的作用在很大程度上是未知的.
研究的目的:
- 调查经过气候变化的花岩中的微生物群落.
- 确定兰酸溶解和利用的生物和遗传机制.
主要方法:
- 采集经过气候变化的花岩和相关土壤的样本.
- 136个微生物基因组的基因组重建.
- 对参与兰化物代谢的基因集群的分析.
主要成果:
- 基于兰化物的甲醇代谢基因集群 (xoxF3,xoxF5) 在温和的花岩中很常见.
- 在Verrucomicrobia,Acidobacteria,Gemmatimonadetes和Alphaproteobacteria中发现了新的xoxF3系统.
- 在细菌中普遍存在的候选金属生物合成系统,特别是酸性细菌.
结论:
- 酸盐矿物溶解,金属生产和化物利用同时发生在花岩气候区.
- 这些微生物过程可能会加速岩石转化为土壤.
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